Paleosismoloji, determines the traces of the old earthquakes on a fault. When this method is applied as a visual and observational, it is limited to the information provided by sedimentolojik and geomorphologic environment which include precipitation, erosion and the effects of ground motion.
Right place selection in ditch works which have an important place in Paleosismolojik researchs, is really difficult on the regions which fault is buried in or deleted because of erosion. GPR is a very effective method for determining the place in ditch Works. GPR method can catch characteristic reflections due to changes like differences in electrical properties, differences in grain size(clay, sand, silt, etc.), space ratio and water content. In this way, GPR can display reflections obtained from stratigraphic layers or fault planes. Esiar, faster and high-resolution measurements can be performed due to new model protected GPR antenna.
